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METHOD FOR EVALUATING THE SEDIMENTARY RATE CONTENT OF ORGANIC MATTER FROM DATA RECORDED IN WELLS BY DIAGRAPHY PROBES

机译:用图谱法从井中记录的数据中估算有机质沉积速率的方法

摘要

Method for determining the content of sedimentary rocks in organic matter from data recorded in a well by at least two logging probes measuring different parameters. / P P The two probes are chosen one to respond in the same meaning to a variation of the water content and organic matter of rocks, the other to respond very differently to a variation of one or the other of these same constituents and, both so that the lines I of organic matter iso-content in a three-pole diagram, are substantially confused that the third pole is the PE water pole or the PA clay pole. The location of the line I 0% is experimentally determined and the organic matter content corresponding to each pair of values of the parameters measured in the well is deduced therefrom. In a diagram where the parameters used depend, for example, on the DELTAT transit time of the sound in the rock and the electrical resistivity Rt of the formations, the iso-content lines constitute a family of parallel lines. / P Application to the study of sedimentary basins.
机译:通过至少两个测量不同参数的测井探针从井中记录的数据中确定有机物中沉积岩含量的方法。

选择了两个探针,一个对岩石的水分和有机质的变化具有相同的含义,另一个对这些相同成分中的一个或另一个的变化具有非常不同的响应并且,两者都使得三极图中有机物等含量线I基本上混淆了,第三极是PE水极或PA粘土极。通过实验确定I 0%线的位置,并据此推导对应于在井中测得的参数的每对值的有机物含量。在使用的参数取决于例如岩石中声音的DELTAT传播时间和地层的电阻率Rt的图表中,等含量线构成了一组平行线。 <在沉积盆地研究中的应用。

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